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المرحلة 4
أستاذ المادة غالب عبد الوهاب علي عباس الدهش
28/02/2016 19:25:55
We have so far discussed the symmetry present in patterns, crystals, and the physical laws. If symmetry is understood as something that limits the number of possible forms of matter and there can be no existence beyond that boundary defined by this symmetrical world, then it can be found that it is not totally correct. Actually, there is almost no existence of a matter in perfect symmetrical state, and as a consequence, the symmetry must be treated as no more than ideal norm from which there is always deviation in reality. If this deviation is called asymmetry, then the problem of symmetry–asymmetry must be understood more closely and intimately. Symmetry and asymmetry are two closely related phenomena that exist in nature, in substances, and even in physical laws, and in fact they are so closely interlinked that they must be viewed as two aspects of the same concept. If beautiful gems and crystals found in nature are the representation of symmetrical world, water in its bulk structural form shows total asymmetrical arrangement of its molecules. Therefore, when the aim of the book is to discuss the patterns, crystals, and the symmetry that is manifested by them, it is also necessary to discuss the deviations from symmetry, that is, asymmetry to make it complete or more comprehensive. The symmetry so far discussed in the earlier chapters consists of several “operations,” which when done on the object, the object comes to a stage of self coincidence and there is no difference between the stages before and after the said operations are done. This is due to invariance of these two positions or stages. Now all these symmetries can be regrouped in two broad categories, that is, (1) local order or symmetry and (2) long range order or symmetry depending on the extent of their validity (Fig. 10.1). This violation of the symmetry on the grain boundary results in a different crystal stage of matter known as polycrystalline state. There is marked difference between the physical properties of these two different stages and many of them, which are characteristic of the respective crystal stage, are important for enhancing the utility of the material. It may be emphasized that the difference between the single crystal and polycrystal state of matter is the randomness of the orientation of any particular plane throughout the bulk. Now this randomness of the orientation will increase if the grain sizes become finer, and this will lead to more asymmetry in one hand and more homogeneity of the physical properties of the material on the other. But there lies enough space in “No man’s Land” between these two states of matter. During grain growth state of the heat treatment, the randomness of the orientation of any particular crystal plane will decrease. This is more conveniently achieved by some mechanical processes of deformation. Now, this decrease in the order of randomness of the arrangement of crystallographic planes results in a shift from random orientation to orientation in some preferred direction of the plane. As a result, the homogeneity of physical properties is hampered, giving rise to some heterogeneity in one hand and introduction of some symmetry in otherwise asymmetric stage of matter. This is some times a boon while fabricating some mechanical structure or materials. This phenomena popularly known as “texture” is, however, beyond the scope of discussion of this book and it will suffice if it is mentioned here that this state of material is also a symmetry in the world of asymmetry. Property Single crystalline stage Polycrystalline stage Symmetry Perfect symmetry in ideal crystals The symmetry is maintained within the region known as grain and remains “almost” same but not exactly same within other neighboring grains belonging to same structure or phase, but is totally different if the grains are of different structures or phases Order of arrangement of constituents It remains same both locally and also throughout the bulk It changes at the boundary between two grains Physical properties As the physical properties are direction dependent, a single crystal shows total heterogeneity A polycrystal in this respect shows homogeneous physical properties When close-packed structures mainly like FCC and HCP and also other structures are deformed, first thing that happens is the fragmentation of the grains called domains and polycrystalline materials, then shows more homogeneity, and the lattice is strained. This strained lattice contains higher energy and resists more the deformation and thus inducts hardening. There appear some drastic changes in their diffraction patterns. The stacking arrangement of their close-packed planes also changes and this result in a defected region compared to surrounding and is known as stacking fault. The number of planes required to bring back the sequence into original are the number of faulted planes. Less the number of faulted planes for a type of deformation process, more is the energy required. Materials having more of this energy known as stacking fault energy do not usually get “work hardened” (Fig.10.2). The displacement of 111 plane by the vector b = 1/2[¯ 10¯ 1] in one step, that is, from one A site to next A site requires larger misfit energy and so A ? B ? C ? A is preferred by the two partials b1 and b2, satisfying the relation b = b1 + b2, which is a/2 [¯ 10¯ 1] = a/6 [¯ 211] + a/6 [¯ 1¯ 12]. The above situation may be visualized as follows: A B C A B C A B C ? ? ? ? ? ? A B C B C A B C A 104 10 Asymmetry in Otherwise Symmetrical Matte ? Faulted zone having h c p stacking sequence B C B C. type. Now this faulted region having different stacking sequence does not commensurate with the perfect stacked regions on both sides. This may be seen as an asymmetry introduced in the symmetrical structure. Introduction of symmetry in otherwise asymmetrical structure is also found in “super lattices” discovered in 1923 in AuCu3 alloys and found later to exist in a number of alloys below a temperature known as critical temperature and they are PtCu3, FeNi3, MnNi3, and (MnFe) Ni3 alloys. Ordinarily an alloy of say A and B elements exists in solid solutions wherein the atoms of A and B are arranged randomly in the interstitials. This is the state of affairs in the alloys other than those mentioned above. In these alloys, the random structures are available at an elevated temperature, and when they are cooled down below a particular temperature called critical temperature, an ordered state happens wherein a particular set of lattice sites are occupied periodically by say A atoms and the other particular sites by B atoms. The solution is then said to be ordered and the lattice thus constituted is known by super lattice. This is a sort of disorder–order transformation and is manifested by an extra reflection in X-ray diffraction pattern. This is an important phenomena not only because of the fact that this ordered state exhibits different physical and chemical properties, but it is also an example of asymmetry to symmetry transformation. The long range order that exist in the super lattice of AuCu3 alloys can be explained as follows: In AuCu3 alloys, the occupancy probability for a particular lattice site say by Au atoms is 1/4, then for Cu atoms it will be 3/4 because of the composition, and the unit cell for the disordered and ordered structures will look as given in Fig. 10.3. The view from any side surface of the lattice will demonstrate the super lattice more explicitly. It can be seen from the above figures that in perfectly ordered state the gold atoms occupy the corner positions and the copper atoms the face-centered positions, whereas in the disordered state there is no such regularity and positions in the unit cell are randomly occupied. As both individual structures are cubic and have almost same lattice parameters, there is only a very slight change in lattice parameter in the ordered state and so there is practically no change in the positions of the X diffraction lines. But the change in the positions of the atoms cause change in the diffracted intensities. Let us see how it changes. In the disordered state the structure factor F can be calculated as follows: fav. = (atomic fraction of Au) fAu+ (atomic fraction of Cu) fCu, fav. = 1/4fAu + 3/3fCu. The positions of the atoms in the unit cell are 000, 1/21/20, 1/201/2, and 01/21/2. The structure factor F = n fne2?i(hxn + kyn + lzn) as there are four atoms in unit cell (n = 4). F = fav 1 + e?i(h+k) + e?i(h+1) + e?i(k+1) For hkl unmixed, F = 4fav. = (fAu + 3fCu) and for hkl mixed F = 0. Therefore, the disordered alloy produces the diffraction pattern similar to face-centered cubic structure. In the ordered state, each unit cell now should contain one Au atom at 000 position and Cu atoms at 1/21/20, 1/201/2, and 01/21/2, and the structure factor then stands out as F = fAu + fCu e?i(h+k) + e?i(h+1) + e?i(k+1) . F = (fAu + 3fCu) when hkl are unmixed, but when hkl are mixed then F instead of being zero it is F = (fAu ? fCu). Therefore, so far as the diffraction lines are concerned, there exists one extra line for the reflection hkl mixed (odd and even) only when the structure is perfectly ordered, otherwise it remains as zero. This extra line is the manifestation of ordered structure and is known as “super lattice line” even though they are weaker than fundamental lines. So, super lattice is a transformation of one “disordered” or asymmetric state to one ordered or symmetric state of this alloy and the order–disorder transformation around a temperature establish that the symmetry and asymmetry may be viewed as the two sides of the same coin. 10.2 A Symmetry in Asymmetry I: Quasi Crystalline State of Matter It has been discussed in earlier Chapters (Chaps.3–5) that a perfect crystalline structure should possess a long range order comprising both translational and rotational symmetries, which should be maintained in three dimensions. However, crystalline order can also be maintained in some ways other than translational symmetry and they are called “aperiodic crystals.” Now, three alternatives to translational symmetry are known: incommensurately modulated crystals, incommensurate composite crystals, and quasi crystals. The modulated structures are obtained from the structures having translational symmetry by giving displacements of the atoms in the periodic structure by equal amounts. Incommensurate composite structures are formed in layered compounds by two interpenetrating periodic structures which are mutually incommensurate. The discovery of quasi crystals has added up one more dimension to crystallography. Influenced by the discovery of a number of quasi crystals or quasi periodic crystals, International Union of Crystallography has redefined the term crystals to mean “any solid having an essentially discrete diffraction diagram.” This broader definition leads to the understanding that microscopic periodicity are sufficient but not necessarily the only condition for crystallinity. A distinct property of quasi crystals that has been found from the diffraction pattern is that it shows fivefold rotation and also other crystallographic point symmetries. We have seen in Chap.3 (Fig.10.3) that there cannot be any crystalline substance with fivefold of symmetry as the motifs having that symmetry cannot make any compact structure, and same is true for sevenfold, eightfold, or tenfold rotation symmetries. It was accepted in classical crystallography
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